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Volcanic hazards:Assessment and monitoring
Christoph Breitkreuz,
TU Bergakademie Freiberg
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Volcanic Hazard – what can be done?
1. Hazard assessment
• Mapping of the volcano and of its products: typical eruption types
• Dating the eruptions: What is the eruption frequency? What are the
periods of dormance?
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Result: Report with hazard map as data base for decision makers during an eruption
Volcanic Hazard – what can be done?
1. Hazard assessment
• Mapping of the volcano and of its products: typical eruption types
• Dating the eruptions: What is the eruption frequency? What are the
periods of dormance?
• Weather conditions and wind directions, depending on seasons and
atmospheric level
• Volcanoes near or at the coast: Tsunami hazards
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Lahar hazard: Mt. Rainier
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2. Monitoring
Initiation of Activity („Volcano awakes“)Monitoring the seismisity (tectonic quakes vs. harmonictremors)Geodesy: change in topography, inflation of volcanic edificeMeasuring the gas composition and flux
Establishing a multi-step alert- and evacuation plan: highest alert level: Eruption within 338 hours (successful at Pinatubo 1991
Monitoring during the ongoing eruptionForecasting the end of eruption > step-wise lowering of alert levels
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Pinatubo 1991:Hazard map*, Seismic Activity*,Satellite monitoirng of atmospheric SO2
*EOS 1991
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Volcanic Ash Advisory Centers: http://www.ssd.noaa.gov/VAAC/
Airplane engine after transit through an ash cloud
Aviation hazard:Monitoring by satellites
Tagesspiegel
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Etna
EOS 75-12 (1994)
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Monitoring vertical movement withInterferometry
Wicks et al. 2002, GRL
Three Sisters, Cascades
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Hawaii Archipel
Hazard of sector collapse-induced tsunamis
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La Palma and her sisters: Tsunami hazard for the Atlantic Ocean
125-136 ka
800-1000 ka
> 900 ka
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Canary Islands: More than 14 large land slides in < 1 Ma (Masson et al. 2002)
Causes:- Volcanic eruption/
magma ascent- Earthquakes- Instability of volcanic edifice
- due to magma intrusion- due to hydrothermal
alteration
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Orsi et al. 2004
Phlegrean Fields west of Naples: Europe most dangerous volcanic region
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Campanian Ignimbrite (37 ka): Sorrent on the southern side of the Bay of Naples